
sedimentary
Yellow Chert (Yellow Jasper)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7. Color: Yellow to brownish-yellow. Luster: Waxy to dull. Crystal Structure: Microcrystalline/Cryptocrystalline (Trigonal). Cleavage: None, conchoidal fracture. Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Color
- Yellow to brownish-yellow
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7. Color: Yellow to brownish-yellow. Luster: Waxy to dull. Crystal Structure: Microcrystalline/Cryptocrystalline (Trigonal). Cleavage: None, conchoidal fracture. Specific Gravity: 2.58-2.91.
Formation & geological history
Formed as a result of the accumulation of microscopic silica fossils (like radiolaria or diatoms) or chemical precipitation from silica-rich fluids in sedimentary basins. Often found in limestone or dolomite formations.
Uses & applications
Historically used for stone tools due to sharp edges when fractured. Currently used for lapidary work, jewelry (cabochons), tumbling, and aggregate in construction.
Geological facts
Yellow chert is often referred to as Yellow Jasper when it is opaque and highly aesthetic. Because it is highly resistant to weathering, it often survives as stream-worn pebbles long after the surrounding rock has eroded.
Field identification & locations
Identify by its waxy luster, conchoidal fracture (smooth, curved breaks), and extreme hardness (cannot be scratched by a steel knife). Commonly found in gravel pits, riverbeds, and beach deposits.
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